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1-20 OF 76 RESULTS FOR
paracoquimbite
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Journal Article
Structure refinements of coquimbite and paracoquimbite from the Hongshan Cu–Au deposit, NW China
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
Published: 01 July 2018
European Journal of Mineralogy (2018) 30 (4): 849–858.
...Zhuming Yang; Gerald Giester The crystal structures of coquimbite and paracoquimbite from the Hongshan Cu–Au deposit, NW China, were refined by single-crystal X-ray diffraction, including the positions of all non-H atoms and hydrogen atoms. The unit-cell parameters of coquimbite are a = 10.9644(15...
Includes: Supplemental Content
Journal Article
Thermodynamic and crystallographic properties of kornelite [Fe 2 (SO 4 ) 3 ·~7.75H 2 O] and paracoquimbite [Fe 2 (SO 4 ) 3 ·9H 2 O]
Sonia Ackermann, Biljana Lazic, Thomas Armbruster, Stephen Doyle, Klaus-Dieter Grevel, Juraj Majzlan
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 November 2009
American Mineralogist (2009) 94 (11-12): 1620–1628.
...Sonia Ackermann; Biljana Lazic; Thomas Armbruster; Stephen Doyle; Klaus-Dieter Grevel; Juraj Majzlan Abstract Enthalpies of formation of kornelite [Fe 2 (SO 4 ) 3 ·~7.75H 2 O] and paracoquimbite [Fe 2 (SO 4 ) 3 ·9H 2 O] were measured by acid (5 N HCl) solution calorimetry at T = 298.15 K...
Journal Article
Crystal Structures and Mineral Chemistry of Hydrated Ferric Sulphates: II. the Crystal Structure of Paracoquimbite
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 October 1971
American Mineralogist (1971) 56 (9-10): 1567–1572.
...Paul D. Robinson; J. H. Fang Abstract The crystal structure of paracoquimbite—Fe 2 (S0 4 ) 3 ·9H 2 O, space group R 3 , a = 10.93 Å, c = 51.30 Å, Z = 12— has been determined by analogy to the structure of coquimbite, and found to differ only in its stacking sequence. Thus the two minerals...
Image
RH– T phase diagram for Fe 2 (SO 4 ) 3 reproduced from Ackermann et al. ...
in Temperature and humidity effects on ferric sulfate stability and phase transformation
> American Mineralogist
Published: 01 February 2012
Figure 6. RH– T phase diagram for Fe 2 (SO 4 ) 3 reproduced from Ackermann et al. (2009) with added observations in this study. The rectangle at 80 °C extending from 20 to 80% RH is the observed transition from paracoquimbite to Fe 2 (SO 4 ) 3 ·5H 2 O. The rectangle from 0 to 10% RH
Image
XRD data showing kornelite transformation to paracoquimbite at 62% RH. Five...
in Humidity-induced phase transitions of ferric sulfate minerals studied by in situ and ex situ X-ray diffraction
> American Mineralogist
Published: 01 November 2009
F igure 10. XRD data showing kornelite transformation to paracoquimbite at 62% RH. Five lines indicate 0, 7, 23, 43, and 79 days preservation of kornelite powders at 62% RH from bottom to top. Percentages are the weight proportions of each phase estimated from Rietveld refinement. K = Kornelite
Image
The crystal structure of paracoquimbite viewed from [1 1 0]. Small red circ...
in Structure refinements of coquimbite and paracoquimbite from the Hongshan Cu–Au deposit, NW China
> European Journal of Mineralogy
Published: 01 July 2018
Fig. 2 The crystal structure of paracoquimbite viewed from [1 1 0]. Small red circle = O; large red circle = O w , gray circle = H.
Image
Comparison of the crystal structures for paracoquimbite (a) and coquimbite ...
in Structure refinements of coquimbite and paracoquimbite from the Hongshan Cu–Au deposit, NW China
> European Journal of Mineralogy
Published: 01 July 2018
Fig. 3 Comparison of the crystal structures for paracoquimbite (a) and coquimbite (b) in blocks both viewed from [1 1 0].
Image
Optical light microscopy images of kornelite ( a ) and paracoquimbite ( b )...
in Thermodynamic and crystallographic properties of kornelite [Fe 2 (SO 4 ) 3 ·~7.75H 2 O] and paracoquimbite [Fe 2 (SO 4 ) 3 ·9H 2 O]
> American Mineralogist
Published: 01 November 2009
F igure 1. Optical light microscopy images of kornelite ( a ) and paracoquimbite ( b ) crystals used for the thermodynamic measurements.
Image
XRD data showing the hydration process of M-Fe 2 (SO 4 ) 3 at 53% RH. Seve...
in Humidity-induced phase transitions of ferric sulfate minerals studied by in situ and ex situ X-ray diffraction
> American Mineralogist
Published: 01 November 2009
F igure 5. XRD data showing the hydration process of M-Fe 2 (SO 4 ) 3 at 53% RH. Several peaks were marked with the initials of corresponding mineral names, either followed by the index numbers in parentheses or not. F = Ferricopiapite; R = Rhomboclase; K = Kornelite; P = Paracoquimbite
Journal Article
Humidity-induced phase transitions of ferric sulfate minerals studied by in situ and ex situ X-ray diffraction
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 November 2009
American Mineralogist (2009) 94 (11-12): 1629–1637.
...F igure 10. XRD data showing kornelite transformation to paracoquimbite at 62% RH. Five lines indicate 0, 7, 23, 43, and 79 days preservation of kornelite powders at 62% RH from bottom to top. Percentages are the weight proportions of each phase estimated from Rietveld refinement. K = Kornelite...
Journal Article
Temperature and humidity effects on ferric sulfate stability and phase transformation
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 February 2012
American Mineralogist (2012) 97 (2-3): 378–383.
...Figure 6. RH– T phase diagram for Fe 2 (SO 4 ) 3 reproduced from Ackermann et al. (2009) with added observations in this study. The rectangle at 80 °C extending from 20 to 80% RH is the observed transition from paracoquimbite to Fe 2 (SO 4 ) 3 ·5H 2 O. The rectangle from 0 to 10% RH...
Image
Results of differential thermal ( a ) and thermogravimetric ( b ) analysis ...
in Thermodynamic and crystallographic properties of kornelite [Fe 2 (SO 4 ) 3 ·~7.75H 2 O] and paracoquimbite [Fe 2 (SO 4 ) 3 ·9H 2 O]
> American Mineralogist
Published: 01 November 2009
F igure 2. Results of differential thermal ( a ) and thermogravimetric ( b ) analysis of the two studied sulfates. The data for kornelite are shown by the solid curve, and those for paracoquimbite are shown by the dashed curve.
Image
Sulfur (S) K -edge k 3 -weighted χ functions ( a ), Fourier transformed ...
in Spectroscopic study on the local structure of sulfate (S O 4 2 − ) incorporated in scorodite (FeAsO 4 ·2H 2 O) lattice: Implications for understanding the Fe(III)-As(V)-S O 4 2 − -bearing minerals formation
> American Mineralogist
Published: 03 October 2022
Figure 9. Sulfur (S) K -edge k 3 -weighted χ functions ( a ), Fourier transformed (FTs)χ functions ( b ), and real part of Fourier transformed EXAFS spectra ( c ) of reference compounds (Na 2 SO 4 and paracoquimbite) and SO 4 -scorodite (1 M Na + and pH 1.2). (Color online.)
Image
XRD data showing the hydration process of T-Fe 2 (SO 4 ) 3 at 53% RH. F = ...
in Humidity-induced phase transitions of ferric sulfate minerals studied by in situ and ex situ X-ray diffraction
> American Mineralogist
Published: 01 November 2009
F igure 7. XRD data showing the hydration process of T-Fe 2 (SO 4 ) 3 at 53% RH. F = Ferricopiapite; R = Rhomboclase; K = Kornelite; P = Paracoquimbite; U = Unknown phase.
Journal Article
Redefinition of coquimbite, AlFe 3+ 3 (SO 4 ) 6 (H 2 O) 12 ⋅6H 2 O
Journal: Mineralogical Magazine
Published: 02 March 2020
Mineralogical Magazine (2020) 84 (2): 275–282.
... the occurrence of Al. Coquimbite has a homeotypic relationship with paracoquimbite, Fe 4 (SO 4 ) 6 (H 2 O) 12 ⋅6H 2 O; both mineral species belong to the coquimbite group. On the contrary, aluminocoquimbite, Al 2 Fe 2 (SO 4 ) 6 (H 2 O) 12 ⋅6H 2 O, has a different topology and does not belong to that group...
Journal Article
Methods to analyze metastable and microparticulate hydrated and hydrous iron sulfate minerals
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 November 2011
American Mineralogist (2011) 96 (11-12): 1856–1869.
... multi-valent and light elements (Fe 2+ , Fe 3+ , OH − , and H 2 O) that may be challenging to quantify. We synthesized or obtained HHIS—szomolnokite, melanterite, rhomboclase, schwertmannite, ferricopiapite, paracoquimbite, and jarosite—as well as Fe-oxides. These nominally pure samples were...
Journal Article
Spectroscopic study on the local structure of sulfate (S O 4 2 − ) incorporated in scorodite (FeAsO 4 ·2H 2 O) lattice: Implications for understanding the Fe(III)-As(V)-S O 4 2 − -bearing minerals formation
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 03 October 2022
American Mineralogist (2022) 107 (10): 1840–1849.
...Figure 9. Sulfur (S) K -edge k 3 -weighted χ functions ( a ), Fourier transformed (FTs)χ functions ( b ), and real part of Fourier transformed EXAFS spectra ( c ) of reference compounds (Na 2 SO 4 and paracoquimbite) and SO 4 -scorodite (1 M Na + and pH 1.2). (Color online.) ...
Journal Article
Crystal structure of synthetic (NH 4 )H 8 Fe (super 3+) 3 (PO 4 ) 6 .6H 2 O
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 June 1979
American Mineralogist (1979) 64 (5-6): 587–592.
...P. B. Moore; T. Araki Abstract Product K, (NH 4 )H 8 Fe 3 3+ (PO 4 ) 6 ·6H 2 O, is based on corner-linking octahedra and tetrahedra and is structurally related to coquimbite, paracoquimbite, and the synthetic Fe 2 (SO 4 ) 3 dimorphs. It is trigonal, а 1 = 9.151(2), с = 16.862(4)A, Z = 2, space...
Image
Sulfur K -edge XANES spectra of ( a ) SO 4 -scorodite (1 M Na + and pH 1....
in Spectroscopic study on the local structure of sulfate (S O 4 2 − ) incorporated in scorodite (FeAsO 4 ·2H 2 O) lattice: Implications for understanding the Fe(III)-As(V)-S O 4 2 − -bearing minerals formation
> American Mineralogist
Published: 03 October 2022
Figure 7. Sulfur K -edge XANES spectra of ( a ) SO 4 -scorodite (1 M Na + and pH 1.2), SO 4 -ferric arsenate, Na 2 SO 4 , and ( b ) the pre-edge features in the S K -edge spectra of römerite, paracoquimbite, jarosite, and SO 4 -scorodite. The continuous energy region above the adsorption edge
Image
XRD patterns of the evolved ferric sulfates at 50 °C. Pattern ( a ) 31% RH,...
in Temperature and humidity effects on ferric sulfate stability and phase transformation
> American Mineralogist
Published: 01 February 2012
for rhomboclase, F for ferricopiapite, K for kornelite, P for paracoquimbite.
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